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  • Red Sea Rift Valley: Plate Tectonics and Divergent Boundaries
    The Red Sea Rift Valley is formed by the Arabian Plate and the African Plate moving apart.

    Here's how it works:

    * Divergent Boundary: The Red Sea is a classic example of a divergent plate boundary. This means the two plates are moving away from each other.

    * Seafloor Spreading: As the plates separate, magma rises from the Earth's mantle and solidifies, creating new oceanic crust. This process is called seafloor spreading.

    * Rift Valley Formation: The continuous separation and creation of new crust results in a depression, or rift valley, along the boundary between the two plates.

    * Red Sea Expansion: The Red Sea continues to widen as the Arabian Plate moves eastward and the African Plate moves westward.

    So, the Red Sea Rift Valley is a direct consequence of the ongoing separation of the Arabian and African plates.

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